Progress report regional geological mapping of the Sungai Katibas area, Sarawak Suhaimi Yusoff
Material type:
TextPublisher: 1993Description: 7p. maps,photos(col.) 30cmSubject(s): Geological mapping -- Sarawak -- Katibas,Sungai | River sediments -- Sarawak -- Katibas,Sungai | Katibas,Sungai(Sarawak)Summary: Sungai Katibas in underlinedby the kapit Members of Belaga Formation. The Kapit member is composed of argillite,shale,phyllite and greywacke,deposited during Paleocene Lower E ocene time (Le ichti et al,1960).The bedding are highly deformed with folding and faulting.Overall, strike of the bedding is WSW-ENE direction with NWW-SSE dipping direction. The lineament analysis shows that the compression force acting on the bedding is in the direction of 170c and 350c
| Item type | Current location | Collection | Call number | Status | Date due | Barcode | Item holds |
|---|---|---|---|---|---|---|---|
| Reports | JMG IBUPEJABAT Open Shelf | Open Shelf | 555.9522 SUH (Browse shelf) | Available | 00003932 |
Browsing JMG IBUPEJABAT shelves, Shelving location: Open Shelf, Collection: Open Shelf Close shelf browser
| 555.9522 RIC Coastal and offshore geoscience activities, 1977, operational centre Sarawak | 555.9522 RIC The northern part of Usun Apau area, Sarawak, Malaysia | 555.9522 RIC 1988 Progress report for 1988 of geological mapping activities | 555.9522 SUH Progress report | 555.9522 ZAI Laporan bersepadu/siap projek | 555.95221 LAMbs Quarry site investigation Bukit Senkujang/Bukit Milas Simunjan, First Division | 555.95221 LAMbt Quarry site investigation, Bukit Tundong, lot 2, block 6, Senggi-Poak Land District, Bau |
Includes bibliographical references
Sungai Katibas in underlinedby the kapit Members of Belaga Formation. The Kapit member is composed of argillite,shale,phyllite and greywacke,deposited during Paleocene Lower E ocene time (Le ichti et al,1960).The bedding are highly deformed with folding and faulting.Overall, strike of the bedding is WSW-ENE direction with NWW-SSE dipping direction. The lineament analysis shows that the compression force acting on the bedding is in the direction of 170c and 350c
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